For example, BC causes an increase
in atmospheric heating, accompanied by a decrease in solar heating of the surface.
Considered either way it is a major player
in atmospheric heating rates.
Together, they describe variations
in atmospheric heat and moisture, and how those translate into weather patterns.
If you were to calculate a change
in atmospheric heat content, that would be closer to your suggestion, and while I don't think it would look much different, it is not the same metric.
I also usually try to include the change in the Relative Humidity, (if it can be found), in my graphs as humidity plays a part
in the atmospheric heat content.
Why didn't you mention the role of aerosols
in atmospheric heat exchanges?
Not all at once of course, but as mentioned above, when the PDO goes positive, we can likely expect a significant change
in the atmospheric heat content as heat energy is transferred from the deep oceans back into the atmosphere.
Interannual variations
in the atmospheric heat budget Kevin E. Trenberth, David P. Stepaniak, and Julie M. Caron JOURNAL OF GEOPHYSICAL RESEARCH, VOL.
Not exact matches
«Clouds are one of the major feedbacks
in cooling and
heating the surface» of the ice, said Nate Miller, an
atmospheric science graduate student at the University of Wisconsin, Madison.
The challenge may arise from the models» inability to adequately represent the
atmospheric heating associated with changes
in cloud populations.
«Volcanic aerosols
in the stratosphere absorb infrared radiation, thereby
heating up the stratosphere, and changing the wind conditions subsequently,» said Dr. Matthew Toohey,
atmospheric scientist at GEOMAR Helmholtz Centre for Ocean Research Kiel.
«I knew just from basic physics that there would be a point at which
heat and humidity would become intolerable, and it didn't seem that anyone had looked at that from a climate change perspective,» says Steven Sherwood, an
atmospheric scientist at the University of New South Wales
in Sydney, Australia.
Knowing what to look for Previous studies investigating
heat wave prediction have looked for patterns
in the tropics, but this research was interesting because the predictive factor is an
atmospheric phenomenon that occurs
in the middle latitudes, Schubert said.
Computer model finds historical patterns
In order to learn that this atmospheric pattern exists in advance of heat waves, Teng and her co-authors had to look far back in the history of heat waves — from before weather records were kep
In order to learn that this
atmospheric pattern exists
in advance of heat waves, Teng and her co-authors had to look far back in the history of heat waves — from before weather records were kep
in advance of
heat waves, Teng and her co-authors had to look far back
in the history of heat waves — from before weather records were kep
in the history of
heat waves — from before weather records were kept.
Of course, the extra
heat trapped by human greenhouse gas emissions is likely to play a bigger role than raindrop friction
in any
atmospheric changes.
Instead of dissipating into space, the infrared radiation that is absorbed by
atmospheric water vapor or carbon dioxide produces
heating, which
in turn makes the earths surface warmer.
«But on top of that, changes
in atmospheric circulation can favor particular weather conditions associated with
heat waves.»
Coumou has examined the waviness of the jet stream
in previous work and has suggested that its large twists and turns, slow - moving undulations called Rossby waves, promote
atmospheric «blocking» — a kind of stagnation of weather patterns that he says can exacerbate
heat waves.
Francesco Panerai of Analytical Mechanical Associates Inc., a materials scientist leading a series of X-ray experiments at Berkeley Lab for NASA Ames Research Center, discusses a 3 - D visualization (shown on screens) of a
heat shield material's microscopic structure
in simulated spacecraft
atmospheric entry conditions.
They created Ti3N4
in a cubic crystalline phase using a laser -
heated diamond anvil cell, which was brought to about 740,000 times normal
atmospheric pressure (74 gigapascals) and about 2,200 degrees Celsius (2,500 kelvin).
That excess tropical energy fueled rising air
in a process known as convection, creating rain, releasing
heat, and forming large - scale
atmospheric patterns called Rossby waves.
NASA Ames Research Center (NASA ARC)
in California's Silicon Valley has traditionally used extreme
heat tests at its Arc Jet Complex to simulate
atmospheric entry conditions.
Scientists finally confirmed this hypothesis
in the 1960s when it became possible to develop adequate models of solar
atmospheric heating.
Using 19 climate models, a team of researchers led by Professor Minghua Zhang of the School of Marine and
Atmospheric Sciences at Stony Brook University, discovered persistent dry and warm biases of simulated climate over the region of the Southern Great Plain
in the central U.S. that was caused by poor modeling of
atmospheric convective systems — the vertical transport of
heat and moisture
in the atmosphere.
The continuation of current trends
in shrub and tree expansion could further amplify this
atmospheric heating by two to seven times.
Another principal investigator for the project, Laura Pan, senior scientist at the National Center for
Atmospheric Research
in Boulder, Colo., believes storm clusters over this area of the Pacific are likely to influence climate
in new ways, especially as the warm ocean temperatures (which feed the storms and chimney) continue to
heat up and
atmospheric patterns continue to evolve.
Sulphur particles
in the stratosphere reflect sunlight and therefore act antagonistically to
atmospheric greenhouse gases like CO2, which capture the
heat of the sun on Earth.
But it is a complicated picture: the effect that extra
atmospheric CO2 has
in these kind of experimental setups might not reflect its effects
in the real world, where other factors — such as elevated
heat, or changes
in precipitation — come into play.
This is due to the unabated upward trends
in human population growth (6),
atmospheric heat content, and OA (2).
In the North Atlantic, more
heat has been retained at deep levels as a result of changes to both the ocean and
atmospheric circulations, which have led to the winter atmosphere extracting less
heat from the ocean.
[NASA's OCO - 2 Mission
in Pictures (Gallery)-RSB- The concentration of
atmospheric carbon dioxide — a
heat - trapping «greenhouse gas» — has risen from 280 parts per million (ppm) before the Industrial Revolution to about 400 ppm today.
The UM Rosenstiel School researchers used historical observations of cloud cover as a proxy for wind velocity
in climate models to analyze the Walker circulation, the
atmospheric air flow and
heat distribution
in the tropic Pacific region that affects patterns of tropical rainfall.
As a result of
atmospheric patterns that both warmed the air and reduced cloud cover as well as increased residual
heat in newly exposed ocean waters, such melting helped open the fabled Northwest Passage for the first time [see photo] this summer and presaged tough times for polar bears and other Arctic animals that rely on sea ice to survive, according to the U.S. Geological Survey.
Scientists have fingerprinted a distinctive
atmospheric wave pattern high above the Northern Hemisphere that can foreshadow the emergence of summertime
heat waves
in the United States more than two weeks
in advance.
That could allow
heat from the ocean to be released into the atmosphere — causing a jump
in atmospheric global warming, Trenberth says: «This could be a very important year.»
Previous studies have hypothesized that the North Pacific
atmospheric ridge is caused by increased ocean surface temperatures and movement of
heat in the tropical Pacific.
All that extra
heat in the Pacific warms the air above, leading to more rising air than normal
in that region, which affects the global
atmospheric circulation.
Increasing
atmospheric CO2 concentrations cause an imbalance
in Earth's
heat budget: more
heat is retained than expelled, which
in turn generates global surface warming.
the Arctic has shown a pattern of strong low - level
atmospheric warming over the Arctic Ocean
in autumn because of
heat loss from the ocean back to the atmosphere....
Because Uranus has no internal source of
heat, its
atmospheric activity was thought to be driven solely by sunlight, which is now weak
in the northern hemisphere.
I am excited about our results because they open a new window on very fundamental processes
in brown dwarfs (
atmospheric circulation,
heat exchanges, and cloud formation) and, at the same time, they also explain a number of past observations that puzzled brown dwarf experts.
Therefore, the strongest motivation for the current scientific review is the need for a synoptic organization of the available knowledge on the field of interactions at different planetary systems,
in parallel with a comparative analysis encompassing the inter-connection among planetary space weather aspects belonging to different disciplines (e.g. plasma variability and its effects on
atmospheric heating).
Gray believes that the increased
atmospheric heat — which he calls a «small warming» — is ``... likely a result of the natural alterations
in global ocean currents which are driven by ocean salinity variations.»
The
atmospheric greenhouse effect, an idea that authors trace back to the traditional works of Fourier 1824, Tyndall 1861, and Arrhenius 1896, and which is still supported
in global climatology, essentially describes a fictitious mechanism,
in which a planetary atmosphere acts as a
heat pump driven by an environment that is radiatively interacting with but radiatively equilibrated to the
atmospheric system.
For example,
in Earth
atmospheric circulation (such as Hadley cells) transport
heat between the warmer equatorial regions to the cool polar regions and this circulation pattern not only determines the temperature distribution, but also sets which regions on Earth are dry or rainy and how clouds form over the planet.
But the burning of oil, coal, and gas also caused most of the historical increase
in atmospheric levels of
heat - trapping greenhouse gases.
For as much as
atmospheric temperatures are rising, the amount of energy being absorbed by the planet is even more striking when one looks into the deep oceans and the change
in the global
heat content (Figure 4).
Changes
in Hadley circulation affects convection and thus
atmospheric moisture content and cloud cover which may
in turn affect net solar
heating as well as the transfer of
heat from Earth to space.
Polar amplification,
in which temperatures at the poles rise more rapidly than temperatures at the equator (due to factors like the global
atmospheric and oceanic circulation of
heat from the equator to the poles), plays a major role
in the rate of ice sheet retreat.
Using
atmospheric data from the last 35 years, study author Daniel Horton, a Stanford University postdoc, and his colleagues found that persistent areas of high pressure
in certain places were linked with extreme
heat waves
in Europe, western Asia and eastern North America.